English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/65337
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

Title

Geochemical and mineralogical characterization of surficial sediments from the Northern Rias: Implications for sediment provenance and impact of the source rocks

AuthorsBernárdez, Patricia ; Prego, R. ; Giralt, Santiago ; Esteve, Jaume; Caetano, Miguel; Parra, Santiago; Francés, G.
KeywordsSurficial sediment
Elemental geochemistry
Mineralogy
Ria
Land-sea exchange
NW Iberian Peninsula
Issue Date2012
PublisherElsevier
CitationMarine Geology 291-294: 63-72 (2012)
AbstractA multidisciplinary study of the elemental geochemistry and mineralogical characteristics of the marine surficial sediment in the Northern Rias (NW Iberian Peninsula) has been carried out. The linkages between the marine sediment composition and their potential sources were examined. The influence of the river-borne sediments is only detected in the innermost part of the three Rias. Regional variations of the mineral assemblages are governed by the source-rock composition of the different geological complexes and the relative source-rock contribution controlled by the continental hydrology. Mineralogical composition of the Ortigueira Ria and adjacent shelf surficial sediments are mainly made up of mafic and ultramafic rocks of the Cape Ortegal complex indicated by the high content of Mg, Mn and chrysotile and riebeckite minerals. In areas nearby Ortegal complex the imprint of heavy minerals present in the surrounding rocks has also been recorded. Barqueiro and Viveiro Rias bed-sediments are influenced by granitic and metamorphic rocks from the Ollo de Sapo complex as revealed by the high contribution of muscovite and quartz. Mining activities in the continental domain left strong imprints on marine surficial sediments. Pyrite content is high in the innermost areas of the Ortigueira Ria since this mineral is exploited in the Mera River basin, whereas high muscovite percentages characterize the Viveiro Ria owing to the abundance of granitic rocks and its exploitation in the Landro River basin. Quartz content is high nearby Cape Estaca de Bares, induced by the presence of an important excavation of this material.
Description10 páginas, 3 tablas, 5 figuras
Publisher version (URL)http://dx.doi.org/10.1016/j.margeo.2011.11.003
URIhttp://hdl.handle.net/10261/65337
DOI10.1016/j.margeo.2011.11.003
ISSN0025-3227
Appears in Collections:(IIM) Artículos
Files in This Item:
File Description SizeFormat 
Geochemical_mineralogical.pdf609,8 kBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.